Chandpur Fm
Type Locality and Naming
Himachal Pradesh-Uttarakhand, Deoban Basin; named after Chandpur village. Kumaun Region; Kumaun, name derived from a peak (30°42':77°40') in southeastern Himachal Pradesh (Auden, 1934). [Original Publication: Auden, J.B., 1934. The Geology of the Krol Belt. Rec. Geol. Surv. India, 67, 357-454.]
Lithology and Thickness
In Deoban Basin, claystone. Fine alternation of shale, siltstone, quartzwacke; ~1250 m. In Kumaun Region, Siltstone. Olive green and grey phyllites interbedded and finely inter-banded with meta-siltstone and very fine-grained wackes, with local meta-volcanic rocks; ~400m.
Relationships and Distribution
Lower contact
Conformable with Mandhali Fm in Deoban Basin, Mandhali rocks (Mandhali Fm) gradually passes into the Chandpur phyllites in Kumaun Region.
Upper contact
Conformable with Nagthat Fm in Deoban Basin, The upper limit in the southern sedimentary belt is unconformity marked by conglomerate purple quartzite of the succeeding Nagthat Fm. (Auden, 1934) in Kumaun Region.
Regional extent
Eastern Himachal and western Uttarakhand in Deoban Basin. The bulk of the Nag Tibba Range in Garhwal from the eastern Nayar to the valley of the Tons and beyond is built up of the Chandpur Fm in Kumaun Region. Forms middle part of Jaunsar Gr, and correlatable to Chhaossa Fm.
GeoJSON
Fossils
None
Age
Depositional setting
Shelf-mud transition zone of a tidal flat complex, with local turbidites.
Additional Information